Coalescing alluvial fanscone-shaped deposits of alluvium that operate with each otherare fashioned exactly where rivers arise in the mountains. If the rivers are significant adequate to increase their courses to the sea, small deltaic plains create before the fans; this occurs most often where by the rivers empty into shallow and sheltered bays, as while in the deltas of Kantō (Kwanto), Nōbi, and Ōsaka.
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One consequence is usually that mountain blocks in many cases are bounded by fault scarps and flexure slopes that descend in action formation towards the adjacent lowlands.